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Landscape Distribution of Microbial Activity in the McMurdo Dry Valleys: Linked Biotic Processes, Hydrology, and Geochemistry in a Cold Desert Ecosystem
Authors:Lydia H Zeglin  Robert L Sinsabaugh  John E Barrett  Michael N Gooseff  Cristina D Takacs-Vesbach
Institution:(1) Department of Biology, MSC03 2020, University of New Mexico, Albuquerque, NM 87131, USA;(2) Present address: Department of Crop and Soil Science, Oregon State University, Corvallis, OR 97331, USA;(3) Department of Biological Sciences, Virginia Polytechnic Institute and State University, Blacksburg, VA 24061, USA;(4) Department of Civil and Environmental Engineering, The Pennsylvania State University, University Park, PA 16802, USA
Abstract:In desert ecosystems, microbial activity and associated nutrient cycles are driven primarily by water availability and secondarily by nutrient availability. This is especially apparent in the extremely low productivity cold deserts of the McMurdo Dry Valleys, Antarctica. In this region, sediments near streams and lakes provide the seasonally wet conditions necessary for microbial activity and nutrient cycling and thus transfer energy to higher organisms. However, aside from a few studies of soil respiration, rates of microbial activity throughout the region remain unexplored. We measured extracellular enzyme activity potentials (alkaline phosphatase, leucine-aminopeptidase, beta-glucosidase, phenol oxidase, and peroxidase) in soils adjacent to lakes and streams, expecting activity to be primarily related to soil water content, as well as time of season and organic matter supply. Phosphatase and beta-glucosidase activities were higher in shoreline than upland soils; however, potential rates were not correlated with soil water content. Instead, soil organic matter, salinity, and pH were the best predictors of microbial activity. Microbial nutrient limitation metrics estimated from extracellular enzyme activity were correlated with pH and salinity and exhibited similar patterns to previously published trends in soil P and N content. Compared to other terrestrial ecosystems, organic matter specific rates for leucine-aminopeptidase and oxidative enzyme activities were high, typical of alkaline desert soils. Phosphatase activity was close to the global mean whereas beta-glucosidase activity was extremely low, which may reflect the lack of vascular plant derived organic matter in the Dry Valleys. In this cold desert ecosystem, water availability promotes microbial activity, and microbial nutrient cycling potentials are related to soil geochemistry. Author contributions:   LHZ performed research, analyzed data, and wrote the paper; RLS contributed new methods and wrote the paper; JEB conceived/designed study, performed research and analyzed data; MNG conceived/designed study and performed research; CTV conceived/designed study and performed research.
Keywords:desert  biogeochemistry  microbial ecology  extracellular enzyme activity  hydrologic margin  McMurdo Dry Valleys
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